La Palma (Spanish:[laˈpalma]ⓘ,locally[lɐˈpɑ(l)mɐ]), also known asLa isla bonita (English:The Beautiful Island) and historicallySan Miguel de La Palma, is the most northwesterly island of theCanary Islands, a Spanishautonomous community andarchipelago inMacaronesia in the North Atlantic Ocean. La Palma has an area of 708.32 square kilometres (273.48 sq mi) making it the fifth largest of the eight main Canary Islands. The total population at the start of 2023 was 84,338,[3][4] of whom 15,522 lived in the capital,Santa Cruz de La Palma and 20,375 inLos Llanos de Aridane. Its highest mountain is theRoque de los Muchachos, at 2,426 metres (7,959 ft), being second among the peaks of the Canaries after theTeide massif onTenerife.
In 1815, the German geologistLeopold von Buch visited the Canary Islands. It was as a result of his visit to Tenerife, where he visited the Las Cañadas caldera, and then later to La Palma, where he visited the Taburiente caldera, that the Spanish word forcauldron or large cooking pot – "caldera" – was introduced into the geological vocabulary. In the center of the island is theCaldera de Taburiente National Park, one of four national parks in the Canary Islands.
The full name of the island is "San Miguel de La Palma" ("Saint Michael of La Palma"), usually abbreviated simply to "La Palma". La Palma is nicknamed "La Isla Bonita" ("beautiful island").[5]
La Palma, like the other islands of the Canary Islands archipelago, is a volcanic ocean island. The volcano rises almost 7 km (4 mi) above the floor of the Atlantic Ocean.[6] There is road access from sea level to the summit at 2,426 m (7,959 ft),[7] which is marked by an outcrop of rocks called Roque de Los Muchachos ("Rock of the Young Men"). This is the site of theRoque de los Muchachos Observatory, one of the world's premier astronomical observatories.[8]
La Palma's geography is a result of thevolcanic formation of the island. The highest peaks reach over 2,400 m (7,874 ft) above sea level, and the base of the island is located almost 4,000 m (13,123 ft) below sea level. The northern part of La Palma is dominated by theCaldera de Taburiente, with a width of 9 km (6 mi) and a depth of 1,500 m (4,921 ft). It is surrounded by a ring of mountains ranging from 1,600 m (5,249 ft) to 2,400 m (7,874 ft) in height. On its northern side is the exposed remains of the originalseamount. Only the deep Barranco de las Angustias ("Ravine of Anxiety") ravine leads into the inner area of the caldera, which is a national park. It can be reached only by hiking. The outer slopes are cut by numerousgorges which run from 2,000 m (6,562 ft) down to the sea. Today, only a few of these carry water due to the manywater tunnels that have been cut into the island's structure.
From the Caldera de Taburiente to the south runs the ridge Cumbre Nueva ('New Ridge', which despite its name is older than theCumbre Vieja, 'Old Ridge.') The southern part of La Palma consists of the Cumbre Vieja, a volcanic ridge formed by numerous volcanic cones built oflava andscoria. The Cumbre Vieja ridge is active, last erupting in the2021 La Palma eruption, which destroyed more than 2600 buildings and caused one death. Beyond Punta de Fuencaliente at the southern tip of the island, the Cumbre Vieja continues in a southerly direction as asubmarine volcano.
Satellite image of La Palma, with theCaldera de Taburiente visible (north is to the lower right)Crater of San Antonio volcano (last erupted 1677)A view of the island looking southPico Birigoyo is the northernmost of the high volcanic peaks along theCumbre ViejaWalls ofCaldera de Taburiente
Like all of the Canary Islands, La Palma originally formed as aseamount throughsubmarine volcanic activity. Along with Tenerife, La Palma is the most volcanically active of the Canary Islands. Its base lies almost 4,000 m (13,123 ft) below sea level and reaches a height of 2,426 m (7,959 ft) above sea level.[9] About a half a million years ago, the Taburiente volcano collapsed with a giantlandslide, forming theCaldera de Taburiente. Erosion has since exposed part of the old seamount in the northern part of the caldera. Since the Spanish have kept records, there have been eight eruptions – all of which have occurred on theCumbre Vieja volcanic ridge:[10]
1470–1492 Montaña Quemada
1585 Tajuya
1646 Volcán Martín
1677 Volcán San Antonio
1712 El Charco
1949 Volcán San Juan: Duraznero, Hoyo Negro and Llano del Banco vents
At Cumbre Vieja ridgea new monogenetic volcano burst on 19 September 2021 after several seismic crises that rocked the island, among other anomalies regarding volcanic surveillance.[11] At 85 days, it is the longest known and the most damaging volcanic eruption on La Palma since records began.[12] The total damage caused by the volcano amounts up to 843 millioneuros.[13]A Special Commissioner for the Reconstruction of the island of La Palma was created in 2022, tasked with coordinating and promoting the actions adopted by theGeneral State Administration to repair the damage caused byvolcanic eruptions and for the reconstruction of the island.[14]Hector Izquierdo Triana, born in La Palma and secretary of state for finance at that time, was appointed to this responsibility.[15][16]
In an episode of theBBCHorizon series broadcast on 12 October 2000, two geologists hypothesised that during a future eruption, the western flank ofCumbre Vieja, with a mass of approximately 1.5 x1015 kg, could slide into the ocean. This could then generate a giant wave, known as a "megatsunami" around 650–900 m (2,130–2,950 ft) high. The wave could radiate out across the Atlantic and inundate much of the eastern seaboard of North America, and many of the islands in theCaribbean and northern coasts of South America between six and eight hours later. They estimate that such a tsunami could have waves possibly 50 m (164 ft) or higher causing massive devastation along the coastlines. Modelling suggests that the tsunami could inundate up to 25 km (16 mi) inland.[17][18] The claim was also explored in a BBC docu-drama calledEnd Day which went through several hypothetical scenarios of disastrous proportions. However, nowhere in their papers do the authors make any claim about the imminent collapse of the flank. Rather, they state that they have modelled the worst-case scenario.
In 2002 the Tsunami Society published a statement stating "... We would like to halt the scaremongering from these unfounded reports..." The major points raised in this report include:
The claim that half of Cumbre Vieja dropped 4 m (13 ft) during the 1949 eruption is erroneous, and contradicted by physical evidence.
No evidence was sought or shown that there is a fault line dividing the island of La Palma.
Physical evidence shows a 4 km (2 mi) long line in the rock, but the models assumed a 25 km (16 mi) line, for which no physical evidence was given. Further, there is no evidence shown that the 4 km (2 mi) long line extends to beneath the surface.
There has never been a megatsunami in the Atlantic Ocean in recorded history.[19]
A geological survey published in 1999 concluded that the western flank is stable with no evidence ofaseismic creep.[20] Other experts agree that thefracture resulting from the 1949 eruption is a shallow and inactive surface expression that should be monitored, but consider the possibility that it is unstable as being almost nonexistent.[21] Also, it is likely that themorphology of the floor of the Atlantic Ocean would hinder the propagation of a transoceanic tsunami.[22] In 2006 Jan Nieuwenhuis ofDelft University of Technology simulated several volcanic eruptions and calculated it would take another 10,000 years for the flanks to become sufficiently high and unstable to cause a massive collapse.[23]
A 2008 paper looked into the worst-case scenario of a massive landslide and subsequent megatsunami. The authors concluded that waves could reach heights in the range 10 to 188 meters in the Canary Islands, but that the waves would dissipate as they radiated out into the Atlantic Ocean. They predict 40 meters height for some nearby island systems. For continents, the worst effects would be expected in Northern Brazil (13.6 m), French Guiana (12.7 m), mid-US (9.6 m), Western Sahara (largest prediction at 37 meters) and Mauritania (9.7 m). While still large, this would not qualify as a megatsunami (apart from locally inMacaronesia), with the highest prediction for Western Sahara comparable to the2011 Japanese tsunami.[24]
La Palma is characterized by two main climate types: the warm/hot summer Mediterranean climate (Köppen: Csb/Csa), characterized by dry summers and humid winters, is prevalent in the northern coast and in the mid to high altitudes of the island. At lower altitudes, particularly at the south and southwest coasts, the climate becomessemi-arid (Köppen: BSh).[25] Average temperatures at the coast vary from 18 °C (64 °F) in January and February to 24 °C (75 °F) in August and September. For a Canary island, the weather is quite cloudy, as La Palma is far more exposed to marine air systems than easterly islands, caused by theCanary Current. As altitude increases moving inland, the climate becomes cooler and more humid, which provides conditions forlaurisilvacloud forests to occur, such as the one in the Natural Park of Bosque de los Tiles.[26]
Black sand beach in Puerto NaosTerraced fields in La Palma
The local economy is primarily based on agriculture and tourism. Bananas are grown throughout the island with many banana farms on the western side of the island in Los Llanos de Aridane. Following the2021 Cumbre Vieja volcanic eruption, studies have shown the volcanic activity did not significantly contaminate banana crops on the island. Other crops includebird of paradise flowers, oranges, avocados and grapes. Local ranchers raise cattle, sheep and goats. Fishermen operating from Santa Cruz de La Palma, Tazacorte, and Puerto Naos catch fish for the local markets.
TheCanary Island pine is found on all of the western Canary Islands, but it is particularly abundant on La Palma. The pine forests are also home to two recently discovered and extremely rare La Palma endemics:Lotus eremiticus andL. pyranthus.
Cytisus supranubius, a white-floweredbroom known locally as Retama del Teide, is native to La Palma and Tenerife, being restricted to the alpine/subalpine habitats present only in these two islands. Like Tenerife, La Palma also has its own alpine violet,Viola palmensis.
Echium pininana is endemic to La Palma and the tallest species in the genus, reaching over 4 m. It is related toEchium wildpretii which occurs, with separate subspecies, in the subalpine zone of both Tenerife and La Palma. Both species aremonocarpic, producing a massive terminalinflorescence.Echium webbii, a branched shrub with several smaller, dark blue flower spikes, is another island endemic with close relatives on Tenerife.
In addition, many other animals have been introduced, including rabbits andBarbary sheep, or aoudads, which have become a serious threat to endemic flora. TheGarafian Sheepdog Breed originates on the island.
Abiosphere reserve was established in 1983, and extended and renamed in 1997 and 2002.[38]
At the time of European colonization, the Canary Islands were inhabited by native Canarians, referred to collectively asGuanches, although the natives of La Palma are more correctly known asAuaritas (SeeCanary Islands in pre-colonial times). The origin of these natives is unclear but they are believed to share common ancestry with theBerbers of North Africa. The Guanches had a Neolithic culture divided into several clans led by chiefs. Their name for La Palma wasBenahoare. The main remnants of this culture are their cave dwellings, enigmaticpetroglyphs and paved stone paths through the mountains. After the Spanish occupation of La Palma, the native Canarians vanished by either being killed, sold into slavery or by assimilating into the Spanish population.
It is believed that theCanary Islands were known to thePhoenicians andGreeks, but the earliest written evidence is by theRoman writerPliny The Elder, who quotedJuba II ofNumidia, but Juba's writings were subsequently lost. TheGenoese navigatorLancelotto Malocello reached the archipelago in 1312 and remained for two decades until expelled by a native uprising. In 1404 the Spaniards began the conquest of the islands. Though the first landing on La Palma was in 1405, it took until 1493 and several bloody battles until the last resistance of the natives was broken. The conqueror of La Palma wasAlonso Fernández de Lugo, who defeatedTanausu, the last king on the island. He ruled the area known as Acero (Caldera de Taburiente). Tanausu was ambushed after agreeing to a truce arranged by Fernández de Lugo and Juan de Palma, a Guanche who had converted to Christianity and who was a relative of Tanausu.
For the next two centuries, settlements on La Palma became rich as the island served as a trading post on the way to theNew World. La Palma received immigrants fromCastile,Majorca, Andalusia,Portugal andCatalonia.
The island is predominately Roman Catholic and since 1676, has been known for the festival ofFiestas Lustrales de la Bajada de la Virgen de las Nieves (the bringing down of theVirgin of the Snow,Virgen de las Nieves), which has a rich history, from the time of the Bishop of the Canaries, Bartolomé García Ximénez. The festival features the dancing of "enanos" or midgets. The costumes that people wear have a hole at the top of the hat to allow them to see out, while giving the appearance of dancing midgets. People come from all over the world for the celebration which happens every five years. The image of the Virgin is taken down from her sanctuary (located in a hilly area on the outskirts ofSanta Cruz de La Palma) and paraded around the city of Santa Cruz with the festival lasting nearly two weeks before she is returned. The last time this event was performed in 2015 and the next will be in 2025, as in 2020 had to be cancelled due to the global pandemic of COVID-19.
The Virgin of the Snow is the patron saint of La Palma. Many women on the island have the name "Nieves" in her honor. Every 5 August the annual festival of the Virgin is celebrated.
La Palma has a road network of some 1,200 km (746 mi). All the main roads are asphalted and in a good state, although there are many sharp bends, some very narrow. In order to reach some small hamlets in the north of the island it is necessary to travel on unpaved roads. A good paved road approximately 180 km (112 mi), circumscribes the island. Several bus routes exist that unite the main settlements on the island.
A road crosses the island fromTazacorte on the west coast tothe capital city on the east coast of the island. This road is a two-lane highway that includes a pair of two-lane tunnels. The older tunnel is shorter (1,100 m (3,609 ft)) and higher than the newer tunnel (2,880 m (9,449 ft)). When traveling from one side of the mountain to the other it is common to enter one side in complete clouds (the east side) and come out to the sunny side (western side). This is due to the clouds not being able to cross the mountains, an effect caused by the counter trade wind.
Theminas galerias (water tunnels) carry water from sources in the highlands to towns, villages and farms. La Palma receives almost all of its water from themar de nubes (sea of clouds) of the northeasttrade winds. The water condenses on the vegetation, from where it runs into the ground. Eventually it collects inside the rock strata, and is then drained via the galerias into aqueducts and pipes for distribution. The galerias have been cut into the rocks over centuries. It is possible to walk alongside many of the aqueducts, a popular activity for tourists (similar to thelevadas ofMadeira). The tour to the Marcos y Corderos waterfall and springs is also popular.
There is an extensive network of irrigation canals in the valley ofLos Llanos de Aridane. These canals carry water from the mountains throughout the valley and allow for the cultivation of bananas, avocados, flowers, and other plants.
Due to the location of the island and the height of its mountains, some 2,400 m (7,874 ft) above sea level, a number of international astronomicalobservatories have been built on theRoque de los Muchachos. The particular geographical position and climate cause clouds to form between 1,000 m (3,281 ft) and 2,000 m (6,562 ft), usually leaving the observatories with a clear sky. Often, the view from the top of the volcano is a sea of clouds covering the eastern part of the island.[8] Telescopes at the observatory include:
The 2024Netflix original Norwegian seriesLa Palma is inspired by the disproved theory[19] about possible catastrophic events[17] that could happen on the island.[44]
^abc"Estadística del Territorio" [Territory Statistics] (in Spanish). Instituto Canario de Estadística (ISTAC).Archived from the original on 13 November 2015. Retrieved14 August 2019.
^abDay, S. J; Carracedo, J. C; Guillou, H. & Gravestock, P; 1999. Recent structural evolution of the Cumbre Vieja volcano, La Palma, Canary Islands: volcanic rift zone re-configuration as a precursor to flank instability. J. Volcanol. Geotherm Res. 94, 135–167.,
^abPararas-Carayannis, G; 2002. Evaluation of the Threat of Mega Tsunami Generation from Postulated Massive Slope Failures of Island Stratovolcanoes on La Palma, Canary Islands, and on The Island of Hawaii, Science of Tsunami Hazards, Vol 20, No.5, pp 251–277.
^Moss, J.L., McGuire, W.J., Page, D., 1999. Ground deformation monitoring of a potential landslide at La Palma, Canary Islands. J. Volcanol. Geotherm. Res. 94, 251–265.
^Carracedo, J. C; Badiola, E. R; Guillou, H; de la Nuez, J; and Pérez Torrado, F. J; 2001. Geology and Volcanology of La Palma and El Hierro, Western Canaries. Estudios Geol. 57, (5–6) 175–273.
^Murty, T. S; Nirupama, N; Nistor, I; and Rao, A. D. 2005. Why the Atlantic Generally cannot generate trans-oceanic tsunamis? ISET J. of Earthquake Tech. Tech. Note., 42, No. 4, pp 227–236.
^Løvholt, F., G. Pedersen, and G. Gisler. "Oceanic propagation of a potential tsunami from the La Palma Island." Journal of Geophysical Research: Oceans 113.C9 (2008).
_La_Palma_%2526_La_Gomera_Islands%2c_Canary_Islands_(cropped).jpg)
.jpg)
.jpg)
.jpg)
_07_ies.jpg)
_03_ies.jpg)
